Applications


MADflow features a range of widely adopted rheological constitutive relationships and has undergone rigorous validation and calibration through extensive laboratory experiments and/or field case history matching, encompassing diverse mass properties. Furthermore, default incorporation of the Mohr–Coulomb failure criterion enhances frictional-based models. Users can manually adjust lateral pressure yield ratios for both active and passive states as needed.

The Manning or Voellmy turbulent effect can be added to either the friction model or visco-plastic models (Bingham or Herschel-Bulkley).

Entrainment and erosion models include linear and power-law formulations, Hanson's hydraulic erosion mechanism and simplified Soulsby-van Rijn sediment transport formula.

Rheology Models

Model Description
Bingham flow shear resistance is a function of the constant Bingham yield stress and Bingham dynamic viscosity.
Coulomb Viscous flow shear resistance is a combination of yield stress, frictional resistance and viscous resistance, which couples particle-particle interaction in a viscous fluid between the intervening lubrication layer of fluid and the deformation of solid particles.
Frictional flow shear resistance is a function of flow depth, coefficient of apparent / dynamic friction (which is a function of shear stress and normal stress).
Herschel-Bulkley flow shear resistance is a function of yield stress, a consistency index, and a flow behavior index associated with shear-thinning or shear-thickening behavior.
Plastic flow shear resistance is controlled by a constant strength, such as residual undrained shear strength of the mobilized material.
Quadratic flow shear resistance consists of Bingham viscous stress and dispersive / turbulent components in a higher order term which is combined into an equivalent Manning’s coefficient.
Sassa flow shear resistance is a function of flow depth, a constant cohesion and an apparent frictional angle.
Voellmy flow shear resistance consists of a frictional term and a turbulent term which relates to flow velocity and a turbulent coefficient, and empirically accounts for possible sources of velocity-dependent resistance during runout.

Selected Technical Papers

All settings for rheological models are region dependent, and MADflow handles the subaerial and subaqueous debris flows or landslides in the same run. NULL regions can also be defined to reduce the overall computational cost or to represent any irregular boundary geometry or non-overtopping objects (e.g. tall buildings) within the flow path.